增强UV-B辐射对高山植物麻花艽净光合速率的影响

在高寒矮嵩草 (K obresia humilis)草甸地区以太阳短波辐射为背景 ,建立了人工增强 U V- B辐射的实验装置 ,每天增补 15 .8k J· m- 2 的辐射剂量 ,模拟平流层臭氧破坏约 5 %时近地表面太阳 UV- B辐射的增强。观测表明 :UV- B辐射的增强对麻花艽 (Gentiana straminea)植物的光合作用无明显的抑制或伤害作用。相反 ,在早晨补充UV- B辐射的短时间内 ,叶片的 Pn 随 Gs的增大而有所提高。随 UV- B辐射时间的延长 ,约在 11∶ 30～ 12∶ 30 ,Pn和Gs有所降低。U V- B辐射时间进一步延长后 (约 14∶ 0 0以后 ) ,处理和对照组叶片 Pn和 Gs的差异趋向不明显。增强太阳 UV- B辐射后 ,麻花艽叶片的光合色素并无明显变化 ,U V-B 吸收物质的含量也无明显变化。麻花艽叶片厚度的直接测量表明: 增强UV -B 辐射能明显提高叶片的厚度。叶片厚度的增加可补偿增强UV -B 辐射后引起的光合色素的光降解, 改善单位叶面积为基础的光合速率, 是高原植物对强UV-B 辐射的一种适应方式。

增强的UV-B辐射对黄瓜（Cucumis sativus）不同叶位叶片生长、光合作用和呼吸作用的影响

在植物生长室中 ,黄瓜植株第 1片真叶出现后 ,用人工UV B光源照射 6 0d ,测定植物各叶位叶片的生长和生理活动 .结果表明 ,UV B辐射条件下 ,植物出叶时间被延迟 ;叶面积和叶干重下降 ,降幅与叶位高低正相关 ;叶片含水量降低 ,老龄叶片 (第 1叶 ,下位叶 )和幼龄叶片 (第 5叶 ,上位叶 )的水分降幅均高于成年叶片 (第 3叶 ,中位叶 ) ;叶片的伸展速度、叶片数目以及单叶面积减少 ,致使黄瓜总叶面积下降 ;植株节间长度缩短 ,是植株矮化的重要原因 ;根、茎、叶等器官之间的相关生长变化不大.叶片生长在其中起重要的协调作用. UV-B 降低Pn和EAQE ,对光合作用的抑制程度随叶位升高而增加. UV-B 辐射后,黄瓜叶片的光呼吸显著提高,增幅与叶片发育阶段有关. UV-B 对黄瓜第1叶的暗呼吸没有影响,第2 、3 叶略微下降,第4 叶显著升高. 分析认为,植株矮化和叶面积减少有利于植物适应UV-B辐射;水分含量和光合作用减少、呼吸作用增强是黄瓜生长受抑制的生理基础。

Influence of grazing intensity on performance of perennial grass mixtures in the alpine region of the Tibetan Plateau

Effects of grazing intensity on leaf photosynthetic rate (Pn), specific leaf area (SLA), individual tiller density, sward leaf area index (LAI), harvested herbage DM, and species composition in grass mixtures (Clinelymus nutans + Bromus inermis, Elymus nutans + Bromus inermis + Agropyron cristatum and Elymus nutans + Clinelymus nutans + Bromus inermis + Agropyron cristatum) were studied in the alpine region of the Tibetan Plateau. Four grazing intensities (GI), expressed as feed utilisation rates (UR) by Tibetan lambs were imposed as follows: (1) no grazing; (2) 30% UR as light grazing; (3) 50% UR as medium grazing; and (4) 70% UR as high grazing. Leaf Pn rate and tiller density of grasses increased (P < 0.05), while sward LAI and harvested herbage DM declined (P < 0.05) with the increments of GI, although no effect of GI on SLA was observed. With increasing GI, Elymus nutans and Clinelymus nutans increased but Bromus inermis and Agropyron cristatum decreased in swards, LAI and DM contribution. Whether being grazed or not, Elymus nutans + Clinelymus nutans + Bromus inermis + Agropyron cristatum was the most productive sward among the grass mixtures. Thus, two well-performed grass species (Elymus nutans and Clinelymus nutans) and the most productive mixture of four species should be investigated further as the new feed resources in the alpine grazing system of the Tibetan Plateau. Light grazing intensity of 30% UR was recommended for these grass mixtures when swards, LAI, herbage DM harvested, and species compatibility were taken into account.

地震层析成像与天山地区的壳幔深部结构研究

The Tien Shan is the most prominent intracontinental mountain belt on the earth. The active crustal deformation and earthquake activities provide an excellent place to study the continental geodynamics of intracontinental mountain belt. The studies of deep structures in crust and upper mantle are significantly meaningful for understanding the geological evolution and geodynamics of global intracontinental mountain belts. This dissertation focuses on the deep structures and geodynamics in the crust and upper mantle in the Tien Shan mountain belt. With the arrival time data from permanent and temporal seismic stations located in the western and central Tien Shan, using seismic travel time tomographic method, we inversed the P-wave velocity and Vp/Vs structures in the crust and uppermost mantle, the Pn and Sn velocities and Pn anisotropic structures in the uppermost mantle, and the P-wave velocity structures in the crust and mantle deep to 690km depth beneath the Tien Shan. The tomographic results suggest that the deep structures and geodynamics have significant impacts not only on the deformations and earthquake activities in the crust, but also on the mountain building, collision, and dynamics of the whole Tien Shan mountain belt. With the strongly collision and deformations in the crust, the 3-D P-wave velocity and Vp/Vs ratio structures are highly complex. The Pn and Sn velocities in the uppermost mantle beneath the Tien Shan, specially beneath the central Tien Shan, are significantly lower than the seismic wavespeed beneath geological stable regions. We infer that the hot upper mantle from the small-scale convection could elevate the temperature in the lower crust and uppermost mantle, and partially melt the materials in the lower crust. The observations of low P-wave and S-wave velocities, high Vp/Vs ratios near the Moho and the absences of earthquake activities in the lower crust are consistent with this inference. Based on teleseismic tomography images of the upper mantle beneath the Tien Shan, we infer that the lithosphere beneath the Tarim basin has subducted under the Tien Shan to depths as great as 500 km. The lithosphere beneath the Kazakh shield may have subducted to similar depths in the opposite direction, but the limited resolution of this data set makes this inference less certain. These images support the plate boundary model of converge for the Tien Shan, as the lithospheres to the north and south of the range both appear to behave as plates.

ω循环型预条件矩阵及其应用

In this paper, we apply the preconditioned conjugate gradient method to the solution of positive-definite Toeplitz systems, especially we introduce a new kind of co-circulant preconditioners Pn[ca] by the use of embedding method. We have also discussed the properties of these new preconditioners and proved that many of former preconditioners can be considered as some special cases of Pn[co\. Because of the introduction of co-circulant preconditioners pn[a>], we can greatly overcome the singularity caused by circulant preconditioners. We have discussed the oo-circulant series and functions. We compare the ordinary circularity with the co-circularity, showing that the latter one can be considered as the extended form of the former one; correspondingly, many methods and theorems of the ordinary circularity can be extended. Furthermore, we present the co-circulant decompositional method. By the use of this method, we can divide any co-circulant signal into a summation of many sub-signals; especially among those sub-signals, there are many subseries of which their period is just equal to 1, which are actually the frequency elements of the original co-circulant signal. In this way, we can establish the relationship between the signal and its frequency elements, that is, the frequency elements hi the frequency domain are actually signals with the period of 1 in the spatial domain. We have also proved that the co-circulant has already existed in the traditional Fourier theory. By the use of different criteria for constructing preconditioners, we can get many different preconditioned systems. From the preconditioned systems PN[

In situ study of carbon nanotube formation by C2H2 decomposition on an iron-based catalyst

The properties and formation of nanotubes have been extensively studied, but very few deal with the catalytic production mechanism of nanotubes. Two different techniques, thermogravimetric analysis and UV-Raman, have been applied to analyse the carbon deposition by catalysed decomposition of acetylene over an iron-based catalyst. The nature of the produced carbon materials depends on reaction temperature. Also, TEM allows identification of carbon nanotubes, encapsulated particles, and other nanostructures, while UV-Raman confirms its graphitic and graphite-like nature. (C) 2000 Elsevier Science Ltd. All rights reserved.